Integrating geological and multimethod geophysical data can help identify prospective areas for granite-related tungsten mineralization, such as unexposed granitic cupolas and anomalous low-resistivity zones associated with faulted corridors and geochemical anomalies.
The OSIRIS-REx sample return capsule re-entry provided an unprecedented opportunity for a large-scale, multi-institutional geophysical observational campaign, yielding invaluable data on meteor-generated shock waves and atmospheric dynamics.
Crustal thickness at the ultraslow-spreading Gakkel Ridge in the Arctic Ocean varies significantly, ranging from 3.3 km to 8.9 km, and has increased over the past 5 million years, contradicting predictions of passive mantle upwelling models.
Fault network geometry significantly influences earthquake frictional behavior, with simpler fault geometries facilitating smooth fault creep and complex geometries promoting stick-slip earthquakes.
Seismological data shows that the subduction zone seismogenic interface is composed of a network of simultaneously active, metres-thick faults, which influences afterslip propagation and earthquake rupture dynamics.
提案された3D拡散モデルは、入力ガイダンスと制約を組み合わせて複雑な3D地震データを再構築することができます。
A novel diffusion model tailored for 3D seismic data reconstruction with guided sampling and constraint incorporation.